Polar Science,
Journal Year:
2018,
Volume and Issue:
21, P. 6 - 13
Published: Nov. 27, 2018
This
article
provides
a
synthesis
of
the
latest
observational
trends
and
projections
for
future
Arctic.
First,
Arctic
is
already
changing
rapidly
as
result
climate
change.
Contemporary
warm
temperatures
large
sea
ice
deficits
(75%
volume
loss)
demonstrate
states
outside
previous
experience.
Modeled
changes
cryosphere
that
even
limiting
global
temperature
increases
to
near
2
°C
will
leave
much
different
environment
by
mid-century
with
less
snow
ice,
melted
permafrost,
altered
ecosystems,
projected
annual
mean
increase
+4
°C.
Second,
under
ambitious
emission
reduction
scenarios,
high-latitude
land
melt,
including
Greenland,
are
foreseen
continue
due
internal
lags,
leading
accelerating
level
rise
throughout
century.
Third,
may
in
turn
impact
lower
latitudes
through
tundra
greenhouse
gas
release
shifts
ocean
atmospheric
circulation.
Arctic-specific
radiative
heat
storage
feedbacks
become
an
obstacle
achieving
stabilized
climate.
In
light
these
trends,
precautionary
principle
calls
early
adaptation
mitigation
actions.
Bulletin of the American Meteorological Society,
Journal Year:
2013,
Volume and Issue:
94(9), P. 1339 - 1360
Published: July 15, 2013
The
Community
Earth
System
Model
(CESM)
is
a
flexible
and
extensible
community
tool
used
to
investigate
diverse
set
of
system
interactions
across
multiple
time
space
scales.
This
global
coupled
model
significantly
extends
its
predecessor,
the
Climate
Model,
by
incorporating
new
simulation
capabilities.
These
comprise
ability
simulate
biogeochemical
cycles,
including
those
carbon
nitrogen,
variety
atmospheric
chemistry
options,
Greenland
Ice
Sheet,
an
atmosphere
that
lower
thermosphere.
other
capabilities
are
enabling
investigations
into
wide
range
pressing
scientific
questions,
providing
foresight
possible
future
climates
increasing
our
collective
knowledge
about
behavior
system.
Simulations
with
numerous
configurations
CESM
have
been
provided
phase
5
Coupled
Intercomparison
Project
(CMIP5)
being
analyzed
broad
scientists.
Additionally,
source
code
associated
documentation
freely
available
use
for
studies,
making
it
true
tool.
article
describes
this
various
configurations,
highlights
number
Abstract
In
recent
decades,
the
warming
in
Arctic
has
been
much
faster
than
rest
of
world,
a
phenomenon
known
as
amplification.
Numerous
studies
report
that
is
either
twice,
more
or
even
three
times
fast
globe
on
average.
Here
we
show,
by
using
several
observational
datasets
which
cover
region,
during
last
43
years
nearly
four
globe,
higher
ratio
generally
reported
literature.
We
compared
observed
amplification
with
simulated
state-of-the-art
climate
models,
and
found
four-fold
over
1979–2021
an
extremely
rare
occasion
model
simulations.
The
ratios
are
consistent
each
other
if
calculated
longer
period;
however
comparison
obscured
uncertainties
before
1979.
Our
results
indicate
unlikely
event,
models
systematically
tend
to
underestimate
Environmental Research Letters,
Journal Year:
2018,
Volume and Issue:
13(10), P. 103001 - 103001
Published: Sept. 3, 2018
The
decline
in
the
floating
sea
ice
cover
Arctic
is
one
of
most
striking
manifestations
climate
change.
In
this
review,
we
examine
ongoing
loss
across
all
seasons.
Our
analysis
based
on
satellite
retrievals,
atmospheric
reanalysis,
climate-model
simulations
and
a
literature
review.
We
find
that
relative
to
1981–2010
reference
period,
recent
anomalies
spring
winter
coverage
have
been
more
significant
than
any
observed
drop
summer
extent
(SIE)
throughout
period.
For
example,
SIE
May
November
2016
was
almost
four
standard
deviations
below
these
months.
Decadal
during
months
has
accelerated
from
−2.4
%/decade
1979
1999
−3.4%/decade
2000
onwards.
also
regional
for
given
region,
seasonal
larger
closer
region
outer
edge
cover.
Finally,
months,
identify
robust
linear
relationship
between
pan-Arctic
total
anthropogenic
CO2
emissions.
annual
cycle
per
ton
emissions
ranges
slightly
above
1
m2
3
summer.
Based
extrapolation
trends,
Ocean
will
become
sea-ice
free
August
September
an
additional
800
±
300
Gt
emissions,
while
it
becomes
July
October
1400
Journal of the Meteorological Society of Japan Ser II,
Journal Year:
2019,
Volume and Issue:
97(5), P. 931 - 965
Published: Jan. 1, 2019
The
new
Meteorological
Research
Institute
Earth
System
Model
version
2.0
(MRI-ESM2.0)
has
been
developed
based
on
previous
models,
MRI-CGCM3
and
MRI-ESM1,
which
participated
in
the
fifth
phase
of
Coupled
Intercomparison
Project
(CMIP5).
These
models
underwent
numerous
improvements
meant
for
highly
accurate
climate
reproducibility.
This
paper
describes
model
formulation
updates
evaluates
basic
performance
its
physical
components.
nominal
horizontal
resolutions
100
km
atmosphere
ocean
components,
similar
to
models.
atmospheric
vertical
resolution
is
80
layers,
enhanced
from
48
layers
predecessor.
Accumulation
various
concerning
clouds,
such
as
a
stratocumulus
cloud
scheme,
led
remarkable
reduction
errors
shortwave,
longwave,
net
radiation
at
top
atmosphere.
resulting
are
sufficiently
small
compared
with
those
CMIP5
improved
distribution
brings
meridional
heat
transport
required
contributes
reduced
surface
air
temperature
(SAT)
bias.
MRI-ESM2.0
displays
realistic
reproduction
both
mean
interannual
variability.
For
instance,
stratospheric
quasi-biennial
oscillation
can
now
be
realistically
expressed
through
introduction
non-orographic
gravity
wave
drag
parameterization.
historical
experiment,
reasonably
reproduces
global
SAT
change
recent
decades;
however,
cooling
1950s
1960s
warming
afterward
overestimated
observations.
many
aspects
over
expected
demonstrate
superior
experiments
planned
CMIP6.
Wiley Interdisciplinary Reviews Climate Change,
Journal Year:
2013,
Volume and Issue:
5(1), P. 113 - 128
Published: Sept. 30, 2013
Climate
and
weather
variables
such
as
rainfall,
temperature,
pressure
are
indicators
for
hazards
tropical
cyclones,
floods,
fires.
The
impact
of
these
events
can
be
due
to
a
single
variable
being
in
an
extreme
state,
but
more
often
it
is
the
result
combination
not
all
which
necessarily
extreme.
Here,
or
that
lead
referred
compound
event.
Any
given
event
will
depend
upon
nature
number
physical
variables,
range
spatial
temporal
scales,
strength
dependence
between
processes,
perspective
stakeholder
who
defines
impact.
Modeling
large,
complex,
interdisciplinary
undertaking.
To
facilitate
this
task
we
propose
use
influence
diagrams
defining,
mapping,
analyzing,
modeling,
communicating
risk
Ultimately,
greater
appreciation
further
insight
changed
on
how
risks
associated
with
climate‐related
hazards.
WIREs
Clim
Change
2014,
5:113–128.
doi:
10.1002/wcc.252
This
article
categorized
under:
Models
>
Knowledge
Generation
Assessing
Impacts
Representing
Uncertainty
PLoS ONE,
Journal Year:
2013,
Volume and Issue:
8(12), P. e81648 - e81648
Published: Dec. 3, 2013
We
assess
climate
impacts
of
global
warming
using
ongoing
observations
and
paleoclimate
data.
use
Earth’s
measured
energy
imbalance,
data,
simple
representations
the
carbon
cycle
temperature
to
define
emission
reductions
needed
stabilize
avoid
potentially
disastrous
on
today’s
young
people,
future
generations,
nature.
A
cumulative
industrial-era
limit
∼500
GtC
fossil
fuel
emissions
100
storage
in
biosphere
soil
would
keep
close
Holocene
range
which
humanity
other
species
are
adapted.
Cumulative
∼1000
GtC,
sometimes
associated
with
2°C
warming,
spur
“slow”
feedbacks
eventual
3–4°C
consequences.
Rapid
reduction
is
required
restore
balance
ocean
heat
uptake
that
practically
guarantee
irreversible
effects.
Continuation
high
emissions,
given
current
knowledge
consequences,
be
an
act
extraordinary
witting
intergenerational
injustice.
Responsible
policymaking
requires
a
rising
price
preclude
from
most
remaining
coal
unconventional
fuels
phase
down
conventional
fuels.
Reviews of Geophysics,
Journal Year:
2014,
Volume and Issue:
52(3), P. 185 - 217
Published: May 15, 2014
Sea
ice
in
the
Arctic
is
one
of
most
rapidly
changing
components
global
climate
system.
Over
past
few
decades,
summer
areal
extent
has
declined
over
30%,
and
all
months
show
statistically
significant
declining
trends.
New
satellite
missions
techniques
have
greatly
expanded
information
on
sea
thickness,
but
many
uncertainties
remain
data
long-term
records
are
sparse.
However,
thickness
observations
other
satellite-derived
indicate
a
40%
decline
due
large
part
to
loss
thicker,
older
cover.
The
changes
happening
faster
than
models
projected.
With
continued
increasing
temperatures,
ice-free
conditions
likely
sometime
coming
though
there
substantial
exact
timing
high
interannual
variability
will
as
decreases.
already
having
an
impact
flora
fauna
Arctic.
Some
species
face
challenges
future,
while
new
habitat
open
up
for
species.
also
affecting
people
living
working
Native
communities
facing
their
traditional
ways
life,
opportunities
shipping,
fishing,
natural
resource
extraction.
Significant
progress
been
made
recent
years
understanding
its
role
climate,
ecosystem,
human
activities.
furthering
knowledge
processes,
impacts,
future
evolution
Nature Communications,
Journal Year:
2019,
Volume and Issue:
10(1)
Published: Jan. 4, 2019
Abstract
Warming
in
the
Arctic
has
been
much
faster
than
rest
of
world
both
observations
and
model
simulations,
a
phenomenon
known
as
amplification
(AA)
whose
cause
is
still
under
debate.
By
analyzing
data
here
we
show
that
large
AA
occurs
only
from
October
to
April
over
areas
with
significant
sea-ice
loss.
largely
disappears
when
sea
ice
fixed
or
melts
away.
Periods
larger
are
associated
loss,
models
bigger
loss
produce
AA.
Increased
outgoing
longwave
radiation
heat
fluxes
newly
opened
waters
AA,
whereas
all
other
processes
can
indirectly
contribute
by
melting
sea-ice.
We
conclude
necessary
for
existence
need
simulate
realistically
order
correctly
warming
increasing
CO
2
.
Science,
Journal Year:
2013,
Volume and Issue:
341(6145), P. 519 - 524
Published: Aug. 1, 2013
After
a
decade
with
nine
of
the
lowest
arctic
sea-ice
minima
on
record,
including
historically
low
minimum
in
2012,
we
synthesize
recent
developments
study
ecological
responses
to
decline.
Sea-ice
loss
emerges
as
an
important
driver
marine
and
terrestrial
dynamics,
influencing
productivity,
species
interactions,
population
mixing,
gene
flow,
pathogen
disease
transmission.
Major
challenges
near
future
include
assigning
clearer
attribution
sea
ice
primary
such
especially
systems,
addressing
pressures
arising
from
human
use
coastal
near-shore
areas
diminishes.